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Sedimentology of the ∼3.3 Ga upper Mendon Formation, Barberton Greenstone Belt, South Africa
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文摘

Hemipelagic settling of organic matter was the dominant mode of sedimentation.

Background deposition was punctuated by volcanic inputs and storm deposits.

Oldest Mendon sections record upward-deepening, consistent with rifting hypothesis.

Higher Mendon cycles reflect gradual shoaling.

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